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Abstract: Recent instability of ice rises adjacent to Pine Island Glacier, Antarctica suggests irreversible retreat (AGU25)

Recent instability of ice rises adjacent to Pine Island Glacier, Antarctica suggests irreversible retreat

Kate Winter1, John Woodward2, Rebecca J. Sanderson3, Scott Steven Braddock4, Jonathan Adams5, Keir Nichols6, Rebecca McCerery2, Seth W Campbell4, Dylan H Rood7, Ryan Venturelli8, Brenda L Hall4 and Dr. Joanne Johnson9, (1)Northumbria University Newcastle, Newcastle upon Tyne, UNITED KINGDOM, (2)Northumbria University, Newcastle-Upon-Tyne, United Kingdom, (3)University of Newcastle, Newcastle upon Tyne, United Kingdom, (4)University of Maine, Earth and Climate Sciences and Climate Change Institute, Orono, United States, (5)Université de Lorraine, Lorraine, France, (6)Scottish Universities Environmental Research Centre, Glasgow, United Kingdom, (7)Imperial College London, Department of Earth Science and Engineering, London, United Kingdom, (8)Colorado School of Mines, Geology and Geological Engineering, Golden, United States, (9)NERC British Antarctic Survey, Cambridge, United Kingdom